What fraction of interseismic uplift at subduction zones becomes permanent? Observations from southwestern Washington
Juliet Crider, Western Washington University

Reconciling Baja-BC and Flat Shatsky Conjugate Subduction beneath Western U.S.
Gene Humphreys, University of Oregon

Sodic Amphibole Deformation Mechanisms: Comparing the Condrey Mountain Schist Rock Record with Experimental Data
Carolyn Tewksbury-Christle, Fort Lewis College

New perspectives on subduction processing east of, and correlations across the Straight Creek-Fraser River fault, Central Cascades of Washington State
Peter Davis, Pacific Lutheran University

Geomorphic Evidence of Quaternary Surface Rupture along the Rocky Mountain – Tintina Trench
Theron Finley, University of Victoria

The Structure and Frictional Behavior of Seismogenic Faults along the Northern US East Coast: Insights from the 2024 M4.8 New Jersey Earthquake
Folarin Kolawole, Columbia University

Rheological and inherited structural effects on kinematic partitioning in the Southern Iberian shear zone in the Pulo do Lobo metasedimentary rocks
Dyanna Czeck, University of Wisconsin-Milwaukee

The Rupture Process of Subduction Zone Earthquakes
Gene Humphreys, University of Oregon

The important role of ductile strain for accommodating mass transfer and exhumation in contractional orogens: Case studies from the Salmon River suture zone fold-thrust system and the transpressional western Idaho shear zone
Andrea Richardson, Washington State University

Anisotropy of Magnetic Susceptibility (AMS) Fabrics from the Pulo do Lobo formation affected by the Southern Iberian Shear Zone
E. George Meyer, University of Wisconsin-Milwaukee